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N <br /> HOZ/02- + Fe2+ + W 4 Fe3+ + H2O2 <br /> Where, <br /> H202 = Hydrogen Peroxide, Fez+ = Ferrous Ion, Fe3+ = Ferric Ion, <br /> 011e = Hydroxyl Radicals <br /> The by-products for this process are carbon dioxide and water. <br /> The hydroxyl radical that attacks the carbon-hydrogen and other recalcitrant compounds <br /> such as MTBE. The Fenton's chemistry reaction is highly complex, The iron cycles <br /> between the Fe(II) and Fe(IU) oxidation states yields the hydroxyl radical and other by <br /> products (Suthersan, 2002). Residual H202not used in the oxidation process breaks- <br /> down to water and oxygen in a matter of hours. In addition to the reaction described in <br /> Equation 2, there are also a large number of competing reactions including the free <br /> radical scavengers, most importantly, carbonate and bicarbonate alkalinity, that will <br /> greatly affect the overall reaction scheme. In addition, H2O2 can serve as an oxygen <br /> source for microbes in the subsurface to enhance biodegradation of contaminants. <br /> Although handling hydrogen peroxide and other oxidants requires significant safety <br /> training and planning, the oxidant is effective at remediation of a variety of organic <br /> contaminants and is relatively inexpensive. The reaction time for hydrogen peroxide in <br /> E1 the subsurface is within minutes to at most, hours. Rise in temperatures in the <br /> subsurface illustrates the exothermic nature of the oxidation process. Rapid degradation <br /> of hydrocarbons, solvents and organic compounds is the goal of in-situ chemical <br /> oxidation, not the violent decomposition of hydrogen peroxide which does occur at <br /> elevated reaction temperatures. <br /> ydrogerrperoxide-reacts--in--an-optimal-manner-in-4owe"11--settings with-lowe <br /> alkalinity readings. In some cases, acids are used to lower pH. The end products of <br /> oxidation are carbon dioxide and water. Trace chloride from chlorinated compounds <br /> will likely combine with sodium or calcium ions to form salts or with hydrogen to form <br /> weak acids. Careful evaluation of soil and water chemistry using a bench test (Figure 1) <br /> with soil and water samples is recommended prior to the start of any injection process. <br /> Due to the rapid reaction time, subsurface spacing of injection ports must be relatively <br /> close which is dependent on lithology. Clays and silts which are problematic to <br /> remediate in-situ, typically require 3 to 5 foot spacing, whereas injection ports for clean <br /> sand and gravels can be placed at 10 to 15 foot spacing, which is the case for this site. <br /> For in-situ chemical oxidation, the metal catalyst is usually provided by iron oxides <br /> within the soil or fill material, or added separately as a solubilized iron salt, such as iron <br /> sulfate. In addition, pH adjustment using an acid such as sulfuric acid (H2SO4), <br /> hydrochloric acid (HCl), or others are common since the chemical oxidation is more <br /> rapid and efficient under lower pH conditions (pH 2-4 is optimal). Fenton's chemistry <br /> has been well documented for over 100 years and has been in use in water treatment <br /> plants for over 50 years. The supportive chemical processes which essentially results in <br /> 3 <br />